[HTML][HTML] Comments on “A combined derivation of the integrated and vertically resolved, coupled wave–current equations”
Journal of Physical Oceanography, 2017•journals.ametsoc.org
… The Stokes drift profile adjusts from (left panel) the blue profile to the red profile, as the
water depth changes from 6 to 4 m, as waves propagate from x = −200 to 200 m. This
adjustment is made possible by both vertical and horizontal fluxes of wave momentum and
by the setdown of the wave-averaged surface elevation. … This adjustment is made
possible by both vertical and horizontal fluxes of wave momentum and by the setdown of
the wave-averaged surface elevation. …
water depth changes from 6 to 4 m, as waves propagate from x = −200 to 200 m. This
adjustment is made possible by both vertical and horizontal fluxes of wave momentum and
by the setdown of the wave-averaged surface elevation. … This adjustment is made
possible by both vertical and horizontal fluxes of wave momentum and by the setdown of
the wave-averaged surface elevation. …
Aiki, H., and RJ Greatbatch, 2012: Thickness-weighted mean theory for the effect of surface gravity waves on mean flows in the upper ocean. J. Phys. Oceanogr., 42, 725–747, doi: 10.1175/JPO-D-11-095.1.
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